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• W2168758445 endingPage "1020" @default.
• W2168758445 startingPage "1004" @default.
• W2168758445 abstract "New seismic reflection data from the Grand Banks of Newfoundland and the NewfoundlandBasin add to the growing knowledge of the composition, structure and history of this nonvolcanicmargin. Geophysical imaging is now approaching the extent of that done previouslyon the conjugate margin along Iberia, providing a valuable database for the developmentof rifting models. Two parallel profiles over the shelf platform image deep crustal fabricrepresenting Precambrian or possibly Appalachian deformation as well asMesozoic extension.Progressively more intense extension of continental crust is imaged oceanwards without thehighly reflective detachments frequently seen on profiles off Galicia. A landward-dippingevent ‘L’ is imaged sporadically and appears to be analogous to a similar event on the IberianIAM9 profile. The transition zone is probably exposed serpentinized mantle as interpretedoff the Iberian margin although there appears to be a difference in the character of ridgedevelopment and reflectivity. The distinctive ‘U’ reflection identified previously at the baseof the Newfoundland Basin deep water sedimentary section and recently identified as one ormore thin basalt sills is imaged on newly presented profiles that connect previously publishedprofiles SCR3 and SCR2 showing that ‘U’ is highly regular and continuous except whereinterrupted by basement highs. ‘U’ is also seen to have a major impact on the ability to imageunderlying basement. A full transect beginning over completely unextended continental crustthrough to oceanic crust has provided a data set from which estimates of extension and thepre-rifting location of the present continental edge can be made. Two estimates were obtained;85 km based on faulting and 120 km based on crustal thickness." @default.
• W2168758445 created "2016-06-24" @default.
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• W2168758445 date "2009-08-01" @default.
• W2168758445 modified "2023-10-14" @default.
• W2168758445 title "Structure and development of the southeast Newfoundland continental passive margin: derived from SCREECH Transect 3" @default.
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• W2168758445 doi "https://doi.org/10.1111/j.1365-246x.2009.04162.x" @default.
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